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基于反向传播网络和 3D 亥姆霍兹线圈的与非线性干扰兼容的地磁矢量补偿方法。

A geomagnetic vector compensation method compatible with nonlinear interferences based on back propagation network and 3D Helmholtz coil.

机构信息

College of Intelligence Science and Technology, National University of Defense Technology, Changsha 410073, China.

Naval Research Academy, Beijing 100161, China.

出版信息

Rev Sci Instrum. 2023 Mar 1;94(3):035111. doi: 10.1063/5.0138606.

Abstract

Magnetic interferential compensation plays a vital role in geomagnetic vector measurement applications. Traditional compensation accounts for only the permanent interferences, induced field interferences, and eddy-current interferences. However, nonlinear magnetic interferences are found, which also have a great impact on measurement, and it cannot be fully characterized by a linear compensation model. This paper proposes a new compensation method based on a back propagation neural network, which can reduce the influence of the linear model on compensation accuracy due to its good nonlinear mapping capabilities. The high-quality network training requires representative datasets, yet it is a common problem in the engineering field. To provide adequate data, this paper adopts a 3D Helmholtz coil to restore the magnetic signal of a geomagnetic vector measurement system. A 3D Helmholtz coil is more flexible and practical than the geomagnetic vector measurement system itself when generating abundant data under different postures and applications. Simulations and experiments are both conducted to prove the superiority of the proposed method. According to the experiment, the proposed method can reduce the root mean square errors of north, east, and vertical components and the total intensity from 73.25, 68.54, 70.45, and 101.77 nT to 23.35, 23.58, 27.42, and 29.72 nT, respectively, compared with the traditional method.

摘要

磁干扰补偿在地磁矢量测量应用中起着至关重要的作用。传统的补偿仅考虑了永久干扰、感应场干扰和涡流干扰。然而,发现了非线性磁干扰,它对测量也有很大的影响,并且不能用线性补偿模型完全描述。本文提出了一种基于反向传播神经网络的新补偿方法,由于其良好的非线性映射能力,可以降低线性模型对补偿精度的影响。高质量的网络训练需要有代表性的数据集,但这在工程领域是一个常见的问题。为了提供足够的数据,本文采用了一个 3D 亥姆霍兹线圈来恢复地磁矢量测量系统的磁信号。与地磁矢量测量系统本身相比,3D 亥姆霍兹线圈在不同姿态和应用下生成丰富数据时更加灵活和实用。本文通过仿真和实验证明了所提出方法的优越性。根据实验结果,与传统方法相比,所提出的方法可以将北、东、垂直分量和总强度的均方根误差分别从 73.25、68.54、70.45 和 101.77 nT 降低到 23.35、23.58、27.42 和 29.72 nT。

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